1 Wan Shiming, Li Anchun, Clift P D et al. Development of the East Asian monsoon:Mineralogical and sedimentologic records in the northern South China Sea since 20Ma. Palaeogeography, Palaeoclimatology, Palaeoecology, 2007, 254 (3):561~582
[2]
22 乔培军, 邵 磊, 杨守业. 南海西南部晚更新世以来元素地球化学特征的古环境意义. 海洋地质与第四纪地质, 2006, 26 (4):59~65Qiao Peijun, Shao Lei, Yang Shouye. The plaeoenvironmental significance of the character of the element geochemistry in the southwestern South China Sea since Late Pleistocene. Marine Geology & Quaternary Geology, 2006, 26 (4):59~65
[3]
23 Wei Gangjian, Liu Ying, Li Xianhua et al. Major and trace element variations of the sediments at ODP Site 1144, South China Sea, during the last 230ka and their paleoclimate implications. Palaeogeography, Palaeoclimatology, Palaeoecology, 2004, 212 (3):331~342
[4]
24 刘 坚, 陆红锋, 苏 新等. 南海北部BY1钻孔沉积物元素地球化学特征及其古环境意义. 热带海洋学报, 2012, 31 (5):6~11Liu Jian, Lu Hongfeng, Su Xin et al. Element geochemistry of Core BY1 from the northern South China Sea and its paleoenvironmental implication. Journal of Tropical Oceanography, 2012, 31 (5):6~11
[5]
25 王 成, 龚庆杰, 李 刚等. 从南海沉积物中的主量元素比值变化看沉积物源区化学侵蚀变化. 海洋地质动态, 2007, 23 (1):1~5Wang Cheng, Gong Qingjie, Li Gang et al. Changes of chemical erosion in sediment source area recorded by the variation of major element ratio of South China Sea sediments. Marine Geology Letters, 2007, 23 (1):1~5
[6]
26 Wei Gangjian, Liu Ying, Li Xianhua et al. High-resolution elemental records from the South China Sea and their paleoproductivity implications. Paleoceanography, 2003, 18 (2):1054~1065
[7]
27 青子琪, 刘连文, 郑洪波. 越南岸外夏季上升流区22万年来东亚季风的沉积与地球化学记录. 海洋地质与第四纪地质, 2005, 25 (2):67~72Qing Ziqi, Liu Lianwen, Zheng Hongbo. Sedimentological and geochemical records of East Asian monsoon in summer upwelling region off the coast of Vietnam for the past 220,000 years. Marine Geology & Quaternary Geology, 2005, 25 (2):67~72
[8]
28 孟宪伟, 夏 鹏, 张 俊等. 近1.8Ma以来东亚季风演化与青藏高原隆升关系的南海沉积物常量元素记录. 科学通报, 2010, 55 (34):3328~3332Meng Xianwei, Xia Peng, Zhang Jun et al. Evolution of the East Asian monsoon and its response to uplift of the Tibetan Plateau since 1.8Ma recorded by major elements in sediments of the South China Sea. Chinese Science Bulletin, 2010, 55 (34):3328~3332
[9]
29 汪品先. 古海洋学概论. 上海: 同济大学出版社, 1989. 1~316Wang Pinxian. Introduction to Paleoceanography. Shanghai:Tongji University Press, 1989. 1~316
[10]
30 李学杰, 刘 坚, 陈 芳等. 南海北部晚更新世以来的碳酸盐旋回. 第四纪研究, 2008, 28 (3):431~436Li Xuejie, Liu Jian, Chen Fang et al. Carbonate cycles since Late Pleistocene in the northern South China Sea. Quaternary Sciences, 2008, 28 (3):431~436
[11]
31 汪品先, 闵秋宝, 卞云华等. 十三万年来南海北部陆坡的浮游有孔虫及其古海洋学意义. 地质学报, 1986, 60 (3):215~225Wang Pinxian, Min Qiubao, Bian Yunhua et al. Planktonic foraminifera in the continental slope of the northern South China Sea, during the last 130,000 years and their paleo-oceanographic implications. Acta Geologica Sinica, 1986, 60 (3):215~225
[12]
32 李 丽, 王 慧, 贺 娟等. 南海北部4万年以来有机碳和碳酸盐含量变化及古海洋学意义. 海洋地质与第四纪地质, 2008, 28 (6):79~85Li Li, Wang Hui, He Juan et al. The characterizations and paleoceanographic significance of organic and inorganic carbon in northern South China Sea during past 40ka. Marine Geology & Quaternary Geology, 2009, 28 (6):79~85
[13]
33 卞云华, 汪品先, 郑连福等. 南海北部晚第四纪浮游有孔虫的溶解作用旋回. 见: 业治铮, 汪品先编. 南海晚第四纪古海洋学研究. 青岛: 青岛海洋大学出版社, 1992. 261~273Bian Yunhua, Wang Pinxian, Zheng Lianfu et al. Dissolution cycles of Late Quaternary planktonic foraminifera in the northern South China Sea. In:Ye Zhizheng, Wang Pinxian eds. Late Quaternary Paleoceanography Research for the South China Sea. Qingdao:Qingdao Ocean University Press, 1992. 261~273
[14]
34 Miao Q, Thunell R C, Anderson D M. Glacial-Holocene carbonate dissolution and sea surface temperatures in the South China and Sulu Seas. Paleoceanography, 1994, 9 (2):269~290
[15]
44 Wang Rujian, Clemens S, Huang Baoqi et al. Quaternary palaeoceanographic changes in the northern South China Sea(ODP Site 1146):Radiolarian evidence. Journal of Quaternary Science, 2003, 18 (8):745~756
[16]
45 李家英. 南海北部陆坡ODP1144站位第四纪硅藻及其古环境演变. 地质论评, 2002, 48 (5):542~551Li Jiaying. Quaternary diatoms from the South China Sea, Leg 184, Site 1144 and their palaeoenvironmental evolution. Geological Review, 2002, 48 (5):542~551
[17]
65 Jian Zhimin, Zhao Quanhong, Cheng Xinrong et al. Pliocene-Pleistocene stable isotope and paleoceanographic changes in the northern South China Sea. Palaeogeography, Palaeoclimatology, Palaeoecology, 2003, 193 (3):425~442
[18]
66 Luo Yunli, Sun Xiangjun. Vegetation evolution and its response to climatic change during 3.15~0.67Ma in deep-sea pollen record from northern South China Sea. Chinese Science Bulletin, 2013, 58 (3):364~372
[19]
67 田 军, 汪品先, 成鑫荣. 南沙ODP1143站有孔虫同位素变化对地球轨道驱动的响应. 中国科学(D辑), 2004, 34 (5):452~460Tian Jun, Wang Pinxian, Cheng Xinrong. The response of foraminifera isotope variations to the Earth orbital forcing at Nansha ODP Site 1143. Science in China(Series D), 2004, 34 (5):452~460
[20]
68 马文涛, 田 军, 李前裕. 晚上新世赤道太平洋气候转型和北极冰盖扩张的轨道驱动. 科学通报, 2009, 54 (22):3537~3545Ma Wentao, Tian Jun, Li Qianyu. Astronomically modulated Late Pliocene equatorial Pacific climate transition and Northern Hemisphere ice sheet expansion. Chinese Science Bulletin, 2009, 54 (22):3537~3545
[21]
69 陈国成, 郑洪波, 李建如等. 南海西部陆源沉积粒度组成的控制动力及其反映的东亚季风演化. 科学通报, 2007, 52 (23):2768~2776Chen Guocheng, Zheng Hongbo, Li Jianru et al. Dynamic control on grain-size distribution of terrigenous sediments in the western South China Sea:Implication for East Asian monsoon evolution. Chinese Science Bulletin, 2007, 52 (23):2768~2776
[22]
70 翦知湣, 王律江. 南海晚第四纪表层古生产力与东亚季风变迁. 第四纪研究, 1999,(1):32~40Jian Zhimin, Wang Lvjiang. Late Quaternary surface paleo￣productivity and variations of the East Asian monsoon in the South China Sea. Quaternary Sciences, 1999,(1):32~40
[23]
71 Prell W L, Murray D W, Clemens S C et al. Evolution and variability of the Indian Ocean Summer Monsoon:Evidence from the western Arabian Sea drilling program. In:Synthesis of Results from Scientific Drilling in the Indian Ocean, 1993. 447~469
[24]
2 万世明, 李安春, 胥可辉等. 南海北部中新世以来粘土矿物特征及东亚古季风记录. 地球科学——中国地质大学学报, 2008, 33 (3):289~300Wan Shiming, Li Anchun, Xu Kehui et al. Characteristics of clay minerals in the northern South China Sea and its implications for evolution of East Asian monsoon since Miocene. Earth Science——Journal of China University of Geoscience, 2008, 33 (3):289~300
[25]
3 Wan Shiming, Li Anchun, Jan-Berend W S et al. Grain-size records at ODP Site 1146 from the northern South China Sea:Implications on the East Asian monsoon evolution since 20Ma. Science in China(Series D), 2007, 50 (10):1536~1547
[26]
4 Wei Gangjian, Li Xianhua, Liu Ying et al. Geochemical record of chemical weathering and monsoon climate change since the Early Miocene in the South China Sea. Paleoceanography, 2006, 21 (4):1~11
[27]
5 Wang Rujian, Jian Zhimin, Xiao Wenshen et al. Quaternary biogenic opal records in the South China Sea:Linkages to East Asian monsoon, global ice volume and orbital forcing. Science in China(Series D), 2007, 50 (5):710~724
[28]
6 Jian Zhimin, Huang Baoqi, Kuhnt W et al. Late Quaternary upwelling intensity and East Asian monsoon forcing in the South China Sea. Quaternary Research, 2001, 55 (3):363~370
[29]
7 Sun Xiangjun, Luo Yunli, Huang Fei et al. Deep-sea pollen from the South China Sea:Pleistocene indicators of East Asian monsoon. Marine Geology, 2003, 201 (1):97~118
[30]
8 Tian Jun, Wang Pinxian, Cheng Xinrong et al. Forcing mechanism of the Pleistocene East Asian monsoon variations in a phase perspective. Science in China(Series D), 2005, 48 (10):1708~1717
[31]
9 郑洪波, 陈国成, 谢 昕等. 南海晚第四纪陆源沉积: 粒度组成、动力控制及反映的东亚季风演化. 第四纪研究, 2008, 28 (3):414~424Zheng Hongbo, Chen Guocheng, Xie Xin et al. Grain size distribution and dynamic control of late Quaternary terrigenous sediments in the South China Sea and their implication for East Asian monsoon evolution. Quaternary Sciences, 2008, 28 (3):414~424
[32]
10 金海燕, 翦知湣, 谢 昕等. 南海北部晚第四纪高分辨率元素比值反映的东亚季风演变. 第四纪研究, 2011, 31 (2):207~215Jin Haiyan, Jian Zhimin, Xie Xin et al. Late Quaternary East Asian monsoon evolution recorded by high resolution elemental rations in the northern South China Sea. Quaternary Sciences, 2011, 31 (2):207~215
[33]
11 Oppo D W, Sun Youbin. Amplitude and timing of sea-surface temperature change in the northern South China Sea: Dynamic link to the East Asian monsoon. Geology, 2005, 33 (10):785~788
[34]
12 Zhao Meixun, Huang Chiyue, Wang Chiachun et al. A millennial-scale U37K'' sea-surface temperature record from the South China Sea(8°N) over the last 150 kyr:Monsoon and sea-level influence. Palaeogeography, Palaeoclimatology, Palaeoecology, 2006, 236 (1):39~55
[35]
13 Wang L, Sarnthein M, Erlenkeuser H et al. East Asian Monsoon climate during the Late Pleistocene:High-resolution sediment records from the South China Sea. Marine Geology, 1999, 156 (1):245~284
[36]
14 王世朋, 李永祥, 付少英等. 南海北部陆坡GHE24L柱样沉积物磁性特征及其环境意义. 第四纪研究, 2014, 34 (3):516~527Wang Shipeng, Li Yongxiang, Fu Shaoying et al. Environmental changes as recorded by mineral magnetic properties of sediments from the core GHE24L, South China Sea. Quaternary Sciences, 2014, 34 (3):516~527
[37]
15 翦知湣, 王博士, 乔培军. 南海南部晚第四纪表层海水温度的变化及其与极地冰芯古气候记录的比较. 第四纪研究, 2008, 28 (3):391~398Jian Zhimin, Wang Boshi, Qiao Peijun. Late Quaternary changes of sea surface temperature in the southern South China Sea and their comparison with the paleoclimatic records of polar ice cores. Quaternary Sciences, 2008, 28 (3):391~398
[38]
16 罗运利, 孙湘君. 南海深海沉积物花粉记录的快速气候波动事件. 第四纪研究, 1999,(6):536~540Luo Yunli, Sun Xiangjun. Millennial-scale climatic fluctuations in pollen record of deep sea deposit from South China Sea. Quaternary Sciences, 1999,(6):536~540
[39]
17 Boulay S, Colin C, Trentesaux A et al. Sediment sources and East Asian monsoon intensity over the last 450 ky. mineralogical and geochemical investigations on South China Sea sediments. Palaeogeography, Palaeoclimatology, Palaeoecology, 2005, 228 (3):260~277
[40]
18 贺子丁, 刘志飞, 李建如等. 南海西部54万年以来元素地球化学记录及其反映的古环境演变. 地球科学进展, 2012, 27 (3):327~336He Ziding, Liu Zhifei, Li Jianru et al. Elemental geochemical records in the western South China Sea since 540ka and their paleoenvironmental implications. Advances in Earth Science, 2012, 27 (3):327~336
[41]
19 梅 西, 张训华, 郑洪波等. 南海南部120ka以来元素地球化学记录的东亚夏季风变迁. 矿物岩石地球化学通报, 2010, 29 (2):134~141Mei Xi, Zhang Xunhua, Zheng Hongbo et al. Element geochemistry record in southern South China Sea sediments during the past 120ka and its implications for East Asian summer monsoon variation. Bulletin of Mineralogy, Petrology and Geochemistry, 2010, 29 (2):134~141
[42]
20 Sun Youbin, Wu Feng, Clemens S C et al. Processes controlling the geochemical composition of the South China Sea sediments during the last climatic cycle. Chemical Geology, 2008, 257 (3):240~246
[43]
21 Liu Jianguo, Chen Muhong, Xiang Rong et al. Abrupt change of sediment records in the southern South China Sea during the last glacial period and its environment significance. Quaternary International, 2011, 237 (1):109~122
[44]
35 陈萌莎, 黄宝琦, 钮耀诚等. 南海北部17924站位氧同位素3期古海洋学变化. 第四纪研究, 2011, 31 (2):299~306Chen Mengsha, Huang Baoqi, Niu Yaocheng et al. Paleoceangraphic variations of the northern South China Sea from site 17924 during marine isotope stage 3. Quaternary Sciences, 2011, 31 (2):299~306
[45]
36 Wehausen R, Brumsack H J. Astronomical forcing of the East Asian monsoon mirrored by the composition of Pliocene South China Sea sediments. Earth and Planetary Science Letters, 2002, 201 (3):621~636
[46]
37 Wang P, Prell W L, Blum P et al. Site 1145. In:Proceedings of the Ocean Drilling Program, Initial Reports 184,2000. 1~63
[47]
38 Lisiecki L E, Raymo M E. A Pliocene-Pleistocene stack of 57 globally distributed benthic δ18 O records. Paleoceanography, 2005, 20 , PA1003, doi:10 .1029/2004PA001071
40 李 建, 王汝建. 南海北部一百万年以来的表层古生产力变化: 来自ODP1144 站的蛋白石记录. 地质学报, 2004, 78 (2):228~233Li Jian, Wang Rujian. Paleoproductivity variability of the northern South China Sea during the past 1Ma:The opal record from ODP Site 1144. Acta Geologica Sinica, 2004, 78 (2):228~23
[50]
41 黄宝琦, 翦知湣. 越南岸外晚第四纪上升流与东亚夏季风变迁. 第四纪研究, 1999,(6):518~525Huang Baoqi, Jian Zhimin. Late Quaternary coastal upwelling and variations of the East Asian summer monsoon off the Vietnam coast. Quaternary Sciences, 1999,(6):518~525
[51]
42 Wang Rujian, Li Jian. Quaternary high-resolution opal record and its paleoproductivity implication at ODP Site 1143, southern South China Sea. Chinese Science Bulletin, 2003, 48 (4):363~367
[52]
43 梅 西, 张训华, 郑洪波等. 南海南部50万年以来碳酸钙和有机碳记录及其揭示的东亚夏季风演化. 地球科学——中国地质大学学报, 2010, 35 (1):22~30Mei Xi, Zhang Xunhua, Zheng Hongbo et al.500000-year records of carbonate and organic carbon from the southern South China Sea and implication for East Asian summer monsoon evolution. Earth Science——Journal of China University of Geosciences, 2010, 35 (1):22~30
[53]
46 黄宝琦, 林慧玲. 南海东北部晚第四纪古生产力变化. 海洋地质与第四纪地质, 2000, 20 (2):65~68Huang Baoqi, Lin Huiling. Late Quaternary changes of paleoproductivity in the northern South China Sea. Marine Geology & Quaternary Geology, 2000, 20 (2):65~68
[54]
47 Tamburini F, Adatte T, F？llmi K et al. Investigating the history of East Asian monsoon and climate during the last glacial-interglacial period(0~140000 years): Mineralogy and geochemistry of ODP sites 1143 and 1144, South China Sea. Marine Geology, 2003, 201 (1):147~168
49 金秉福, 林振宏, 季福武. 海洋沉积环境和物源的元素地球化学记录释读. 海洋科学进展, 2003, 21 (1):99~106Jin Bingfu, Lin Zhenhong, Ji fuwu. Interpretation of element geochemical records of marine sedimentary environment and provenance. Advances in Marine Science, 2003, 21 (1):99~106
[57]
50 Wehausen R, Tian J, Brumsack H J et al. Geochemistry of Pliocene sediments from ODP Site 1143(southern South China Sea). Proceedings of the Ocean Drilling Program, Science Results,2003, 184 : 1~25
[58]
51 蒋富清, 李安春, 李铁刚. 冲绳海槽南部柱状沉积物地球化学特征及其古环境意义. 海洋地质与第四纪地质, 2002, 22 (3):11~17Jiang Fuqing, Li Anchun, Li Tiegang. Geochemical characteristics for core sediments of the southern Okinawa trough and its paleoenvironmental implication. Marine Geology & Quaternary Geology, 2002, 22 (3):11~17
[59]
52 刘 伟. 南海北部陆坡MIS 5以来的古环境记录. 北京: 中国地质大学博士毕业论文, 2011. 71~74Liu Wei. Paleoclimatic Records from Northern Slop of South China Sea since the Marine Isotope Stage 5. Beijing:The Doctoral Dissertation of China University of Geoscience, 2011. 71~74
[60]
53 Wei Gangjian, Liu Ying, Li Xianhua et al. Climatic impact on Al, K, Sc and Ti in marine sediments: Evidence from ODP site 1144, South China Sea. Geochemical Journal, 2003, 37 (5):593~602
[61]
54 韦刚健, 刘 颖, 李献华等. 南海沉积物中过剩铝问题的探讨. 矿物岩石地球化学通报, 2003, 22 (1):23~25Wei Gangjian, Liu Ying, Li Xianhua et al. Excess Al in the sediments from South China Sea. Bulletin of Mineralogy, Petrology and Geochemistry, 2003, 22 (1):23~25
[62]
55 李粹中. 南海中部沉积物的元素地球化学特征. 东海海洋, 1987, 5 (1):77~91Li Cuizhong. Geochemistry of elements in surface sediments of the South China Sea basin. Donghai Marine Science, 1987, 5 (1):77~91
[63]
56 陈绍谋, 路秀云, 吴传芝等. 南海北部沉积物的地球化学特征及元素赋存状态的研究. 热带海洋学报, 1986, 5 (4):62~70Chen Shaomou, Lu Xiuyun, Wu Chuanzhi et al. The study of geochemistry characteristics of sediments and forms of existence of elements in northern South China Sea. Tropic Oceanology, 1986, 5 (4):62~70
[64]
57 任景玲, 张桂玲, 刘素美等. 海洋中锰的生物地球化学循环研究. 海洋科学进展, 2012, 30 (3):432~440Ren Jingling, Zhang Guiling, Liu Sumei et al. Review on the study of biogeochemical cycle of manganese in the oceans. Advances in Marine Science, 2012, 30 (3):432~440
[65]
58 汪品先. 十五万年来的南海. 上海: 同济大学出版杜, 1995. 96~114Wang Pinxian. Records from South China Sea since 0.15Ma. Shanghai:Tongji University Press, 1995. 96~114
[66]
59 汪品先. 西太平洋边缘海的冰期碳酸盐旋回. 海洋地质与第四纪地质, 1998, 18 (1):1~11Wang Pinxian. Glacial carbonate cycles in western Pacific marginal seas. Marine Geology & Quaternary Geology, 1998, 18 (1):1~11
[67]
60 孙有斌, 强小科, 孙东怀等. 新近纪以来中国黄土高原的风尘纪录. 地层学杂志, 2001, 25 (2):94~101Sun Youbin, Qiang Xiaoke, Sun Donghuai et al. Eolian record of the Chinese Loess Plateau since the Neogene. Journal of Stratigraphy, 2001, 25 (2):94~101
[68]
61 安芷生, 张培震, 王二七等. 中新世以来我国季风-干旱环境演化与青藏高原的生长. 第四纪研究, 2006, 26 (5):678~693An Zhisheng, Zhang Peizhen, Wang Erqi et al. Changes of the monsoon-arid environment in China and growth of the Tibetan Plateau since the Miocene. Quaternary Sciences, 2006, 26 (5):678~693
[69]
62 孙有斌, 刘青松. 晚上新世-早更新世北太平洋和黄土高原的风尘沉积记录的初步对比. 第四纪研究, 2007, 27 (2):263~269Sun Youbin, Liu Qingsong. Preliminary comparison of eolian depositions in the north Pacific and the Chinese Loess Plateau during the Late Pliocence-Early Pleistocene. Quaternary Sciences, 2007, 27 (2):263~269
[70]
63 黄宝琦, 成鑫荣, 翦知湣等. 晚上新世以来南海北部上部水体结构变化及东亚季风演化. 第四纪研究, 2004, 24 (1):110~115Huang Baoqi, Cheng Xingrong, Jian Zhimin et al. Variations in upper ocean structure in the South China Sea and the evolution of the East Asian monsoon since Late Pliocene. Quaternary Sciences, 2004, 24 (1):110~115
[71]
64 刘志飞, Trentesaux A, Clemens S C等. 南海北坡ODP1146站第四纪粘土矿物记录: 洋流搬运与东亚季风演化. 中国科学(D辑), 2003, 33 (3):271~280Liu Zhifei, Trentesaux A, Clemens S C et al. Quaternary clay mineral record of ODP1146 in the northern South China Sea:Currents transport and East Asian monsoon evolution. Science in China(Series D), 2003, 33 (3):271~280
[72]
72 Wang Pinxian, Clemens S, Beaufort L et al. Evolution and variability of the Asian monsoon system: State of the art and outstanding issues. Quaternary Science Reviews, 2005, 24 (5):595~629
